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Late Quaternary vegetation dynamics from central parts of the Madeira River in Brazil
(Soc Botanica Brasil, 2015-01-01)
The present study reconstructs the paleovegetation of a varzea (seasonally flooded) forest in the central parts of the Madeira River floodplain in Brazil using palynological data. Forty-nine cut-bank sediment samples from ...
Seismic stratigraphy of late Neogene: Quaternary units and evolutionary model in the inner sector of Bahia Blanca estuary (Argentina)
(Pergamon-Elsevier Science Ltd, 2020-12)
The Quaternary sedimentary deposit of the inner sector of Bahía Blanca estuary (BBE), Argentina, was studied using high-resolution seismic profiles, core samples and correlation with continental – marine units outcropping ...
Quaternary shortening at the orogenic front of the Central Andes of Argentina: the Las Peñas Thrust System
(Lyell Collection, 2014-06)
The NNW-trending Las Peñas Thrust System is one of the key structures along the Andean orogenic front between 32°15′ and 32°40′S in the Southern Precordillera of Argentina. This east-verging structure crops out over a ...
Late Quaternary vegetation dynamics from central parts of the Madeira River in Brazil
(Soc Botanica Brasil, 2015)
LIZARDS AND SNAKES (LEPIDOSAURIA, SQUAMATA) FROM THE LATE QUATERNARY OF THE STATE OF CEARA IN NORTHEASTERN BRAZIL
(NATL SPELEOLOGICAL SOCHUNTSVILLE, 2012-12)
We present the first formal report on the squamate assemblage from Parque Nacional de Ubajara. This park contains the most important cave complex in the state of Ceara in northeastern Brazil, called Provincia Espeleologica ...
Biostratigraphy and geochronology of the late Cenozoic of Córdoba Province (central Argentina)
(Pergamon-Elsevier Science Ltd, 2013-03)
In the last twenty years, several geological and stratigraphical studies have been undertaken in Córdoba Province, and they have provided useful bases for biostratigraphic work in the late Cenozoic. However, paleontological ...
Two loess formations of upper quaternary age in the brazilian nordeste
(E Schweizerbartsche Verlags, 2010-06)
Two sedimentary formations of eolian origin, composed of silt and loamy silt occur in the interior of the Brazilian Nordeste, several hundred kilometers to the west of the coast (fig. 1). The area is semiarid, dominated ...